The synergistic effects of ocean acidification and organic metabolism on calcium carbonate (CaCO3) dissolution in coral reef sediments

Ocean acidification (OA) is expected to reduce the net ecosystem calcification (NEC) rates and overall accretion of coral reef ecosystems. However, despite the fact that sediments are the most abundant form of calcium carbonate (CaCO3) in coral reef ecosystems and their dissolution may be more sensi...

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Bibliographic Details
Main Authors: Cyronak, Tyler, Eyre, Bradley D
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Alkalinity
total
flux
Aragonite saturation state
Benthos
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Coast and continental shelf
Dissolution rate
Entire community
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Irradiance
Laboratory experiment
Light
Net dissolution rate of calcium carbonate
Net primary production of oxygen
OA-ICC
Ocean Acidification International Coordination Centre
Oxygen
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Primary production/Photosynthesis
Respiration
Respiration rate
community
Rocky-shore community
Salinity
South Pacific
Temperature
water
Treatment
Tropical
Type
Ocean acidification
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.867130
https://doi.org/10.1594/PANGAEA.867130

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